Below is a geologic structure that illustrates the various principles of relative dating. You will identify the basic principles used in relative geologic dating by dragging labels to their corresponding targets in the image below.

Drag the appropriate labels to their respective targets.

Order the five images below along the timeline based on the sequence of geologic events.

Rank from oldest to youngest.

Principle of Inclusions Principle of Cross cutting Relationships aw of Superposition

Principle of Inclusions Principle of Cross- cutting Relationships Law of Superposition layers are cut by an igneous dike layers are tilted, erosion of tilted surface horizontal layers with ocean water at top layers with inclusions from above and below Inclusions from layers above and below